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- W2013772924 abstract "Summary Surface and buried paleosols on Niwot Ridge in the Front Range of Colorado were analyzed for extractable Fe and Al to determine if their distributions would assist in the interpretation of past and present soil-forming environments. Extractable Fe and Al distributions in surface and buried paleosols suggest that leaching is more pronounced in the older paleosols with a considerable difference in soil-forming environment between Pleistocene interstadial, later Pleistocene, and postglacial paleosols. Using radiocarbon dated buried A horizons it appears that little pyrophosphate-extractable Fe and Al have been translocated downward into these middle-latitude alpine buried paleosols. There is no evidence that the Na-pyrophosphate extractable Fe and Al were affected by degradation of organic matter following burial; however, the data suggest that some amorphous Fe and Al might have been affected by soil water movement over permafrost and by redistribution of preweathered sediments." @default.
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- W2013772924 date "1988-02-01" @default.
- W2013772924 modified "2023-10-16" @default.
- W2013772924 title "Extractable Fe and Al in late Pleistocene and Holocene paleosols on Niwot Ridge, Colorado Front Range" @default.
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- W2013772924 doi "https://doi.org/10.1016/0341-8162(88)90013-6" @default.
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